Logo Tropentag

Tropentag, September 17 - 19, 2013 in Stuttgart-Hohenheim

"Agricultural development within the rural-urban continuum"

Fire History of Conifer Forests of Cerro El PotosÍ, Nuevo LeÓn, Mexico

Marco Aurelio Gonzalez Tagle, Diana Yemilet Avila Flores, Javier Jimenez Perez

Universidad Autónoma de Nuevo León, Dept. of Silviculture, Mexico


Fire is one of the most important ecosystem processes contributing to biodiversity and health, so it is useful to study patterns and changes in fire regimes. The fire regime for the coniferous forests of Cerro El Potosí, located in the Sierra Madre Oriental mountain range in northeastern Mexico, was investigated using fire-scarred trees. The selected area for sampling was a part of the coniferous forests, between 2,900 -3,450 m a.s.l., with a northeast aspect and a slope range of 22-38%. The sampling area covered an area of ≈ 2 km. The forest in the sampling area was composed of species such as Abies vejarii, Pinus strobiformis, Pinus greggii, Pinus hartwegii and Pseudotsuga menziesii. To reconstruct the fire history in the area, we took samples from trees with at least one fire scar. We used chain saws to obtain the samples. We collected total and partial sections of stumps, logs, snags and living trees. In addition data were recorded for each tree such as diameter (DBH), status (live, snag, log and stump), slope, aspect and geographical coordinates. From the 22 collected samples, it was only possible to date 16, with a total of 35 fire scars. The samples used were of Pinus strobiformis and Pinus hartwegii. The oldest scar formed in 1807 and the most recent in 1998. The descriptive statistics calculated for the period of reliability (1888-2011) show that the Mean Fire Interval (MFI) for all fires was 11 years and 15.7 years for the larger fires or those that scarred ≥ 25% of all samples. The trees recorded fires from the late 19th century through the late 20th century. Most of the fires corresponded to the 20th century; the last fire recorded was in 1998. We observed shorter fire return periods until before 1955, with an increase in these intervals for subsequent fire events. There was no significant relationship between fire occurrence and climate variables (precipitation and ENSO), suggesting that for our study area fire occurrence is mostly influenced by anthropogenic activities.

Keywords: Cerro Potosí, ENSO, fire scar, forest fire

Contact Address: Marco Aurelio Gonzalez Tagle, Universidad Autónoma de Nuevo León, Dept. of Silviculture, Apartado Postal #1, 67755 Linares, Mexico, e-mail: marco.gonzalez@web.de

Valid HTML 3.2!